内蒙古巴林右旗上卧尔图铜多金属矿成矿条件简析

Analysis of Inner Mongolia's Shan Woertu on Lie in Ba Linyouqi Flag Copper Polymetallic Metallogenic Conditions

上卧尔图铜多金属矿分别隶属于内蒙古自治区巴林右旗查干沐沦苏木,上卧尔图和舍尔图嘎查所辖。3个矿段均位于大兴安岭西南段末端。矿体主要赋存在大石寨组中段。上卧尔图有色金属矿主要有黄铜矿、方铅矿、闪锌矿,贵重金属矿产有银矿。矿区内围岩蚀变较强烈,主要有硅化、绿泥石化、绿帘石化、碳酸盐化。通过对矿体赋存特征、铅锌矿物的分布特点以及矿体、矿化体的空间展布与围岩蚀变的关系,对该矿区的金属矿成矿条件进行了简单的探讨。为后期探矿奠定了一定的基础条件。

Shang Woertu copper polymetallic belongs to the Inner Mongolia Ba Linyouqi autonomous region Cha Ganmulunsumu, Figure Shang Woertu and She Ertu jurisdiction. Three copper polymetallic ore is located in the Da Xinganling southwest. The orebody mainly occurs in the middle stone vitlage group. Shah Woertu non-ferrous metal mainly on chaleopyrite, galena, sphalerite, silver precious metals. In wall rock alteration is stronger, there are mainly silicification and chloritization, epidotization, carbonatization. This article through to the ore body occurrence characteristics-the distribution characteristics of lead-zinc mine content and spatial distribution of ore bodies and mineralized bodies and the relationship between wall rock alteration, metal metallogenic conditions of the mine area has carried on the simple discussion. Late for prospecting the foundation of a Certain condition.